Examining cloud vertical structure and radiative effects from satellite retrievals and evaluation of CMIP6 scenarios
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Published:2023-07-21
Issue:14
Volume:23
Page:8169-8186
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Luo HaoORCID, Quaas JohannesORCID, Han Yong
Abstract
Abstract. Clouds exhibit a wide range of vertical morphologies that
are regulated by distinct atmospheric dynamics and thermodynamics and are
related to a diversity of microphysical properties and radiative effects. In
this study, the new CERES-CloudSat-CALIPSO-MODIS (CCCM) RelD1 dataset is
used to investigate the morphology and spatial distribution of different
cloud vertical structure (CVS) types during 2007–2010. The combined active
and passive satellites provide a more precise CVS than those only based on passive
imagers or microwave radiometers. We group the clouds into 12 CVS classes
based on how they are located or overlapping in three standard atmospheric
layers with pressure thresholds of 440 and 680 hPa. For each of the 12 CVS
types, the global average cloud radiative effects (CREs) at the top of the
atmosphere, within the atmosphere and at the surface, as well as the cloud
heating rate (CHR) profiles are examined. The observations are subsequently
used to evaluate the variations in total, high-, middle- and low-level cloud
fractions in CMIP6 models. The “historical” experiment during 1850–2014 and
two scenarios (ssp245 and ssp585) during 2015–2100 are analyzed. The
observational results show a substantial difference in the spatial pattern
among different CVS types, with the greatest contrast between high and low
clouds. Single-layer cloud fraction is almost 4 times larger on average
than multi-layer cloud fraction, with significant geographic differences associated
with clearly distinguishable regimes, showing that overlapping clouds are
regionally confined. The global average CREs reveal that four types of CVSs
warm the planet, while eight of them cool it. The longwave component drives
the net CHR profile, and the CHR profiles of multi-layer clouds are more
curved and intricate than those of single-layer clouds, resulting in complex
thermal stratifications. According to the long-term analysis from CMIP6, the
projected total cloud fraction decreases faster over land than over the
ocean. The high clouds over the ocean increase significantly, but other
types of clouds over land and the ocean continue to decrease, helping to offset
the decrease in oceanic total cloud fraction. Moreover, it is concluded that
the spatial pattern of CVS types may not be significantly altered by climate
change, and only the cloud fraction is influenced. Our findings suggest that
long-term observed CVS should be emphasized in the future to better
understand CVS responses to anthropogenic forcing and climate change.
Funder
National Natural Science Foundation of China Southern Marine Science and Engineering Guangdong Laboratory China Scholarship Council
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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